On the deep general circulation in the western North Atlantic

dc.contributor.author Schmitz, William J.
dc.date.accessioned 2018-09-24T17:33:28Z
dc.date.available 2018-09-24T17:33:28Z
dc.date.issued 1978-04
dc.description Also published as: Journal of Marine Research, Volume 35, 1977, pp. 21-28 en_US
dc.description.abstract Very large (5-10 cm s-1) long-term averaged zonal flows have been observed near 4000 m depth in the vicinity of a recently hypothesized (Worthington, in press) horizontally restricted subtropical gyre in the deep western North Atlantic. The Reynolds stresses associated with low frequency fluctuations may play a significant role in the dynamics of this deep mean flow, possibly inducing a significant downstream increase in transport of the Gulf Stream, perhaps driving the deep gyre. en_US
dc.description.sponsorship Prepared for the Office of Naval Research under Contracts N00014-66-C-0241; NR 083- 004 and N00014-74-C-0262; NR 083-004 and for the International Decade of Ocean Exploration of the National Science Foundation under Grant OCE75-03962. en_US
dc.identifier.citation Schmitz, W. J. (1978). On the deep general circulation in the western North Atlantic. Woods Hole Oceanographic Institution. https://doi.org/10.1575/1912/10589
dc.identifier.doi 10.1575/1912/10589
dc.identifier.uri https://hdl.handle.net/1912/10589
dc.language.iso en_US en_US
dc.publisher Woods Hole Oceanographic Institution en_US
dc.relation.ispartofseries WHOI Technical Reports en_US
dc.relation.ispartofseries WHOI-78-3 en_US
dc.subject Ocean circulation en_US
dc.title On the deep general circulation in the western North Atlantic en_US
dc.type Technical Report en_US
dspace.entity.type Publication
relation.isAuthorOfPublication 5412bdba-589d-42ee-aa92-611d19722472
relation.isAuthorOfPublication.latestForDiscovery 5412bdba-589d-42ee-aa92-611d19722472
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